摘要
Analyzing the mobile gravity observational data in North China from 2005 and 2009 systematically and deeply, the authors derived dynamic variation of the regional gravity field in different time scales before and after Wen’an MS5.1 earthquake, and studied the relationship between gravity anomaly variation and seismic activity. The result showed that there existed regional gravity anomaly in a wide range in the survey area during the preparation of Wen’an MS5.1 earthquake, and there were local gravity anomaly area and high gradient zone of gravity variation referential to the earthquake preparation. The dynamic image of gravity field clearly reflected the evolution orderly and seismic activity of regional gravity field.